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Walk west to the next stop to see the reddish sediment called terra rossa on the cliff. There are three sinkholes that have eroded walls facing south. Look for more brownish sediments in the shape of an open V on top of the reddish sediments. These formations are believed to be paleochannels. Walk west to the next stop. The reddish sediment that can be seen on the cliff is called terra rossa. In this location, three coalescing sinkholes can be seen, whose external walls facing south have been eroded. Observe the cliff and check for more brownish sediments, in the shape of an open V, which are found on top of the reddish sediments. These formations are interpreted to be paleochannels.